Engineering topics
Smrekar, Suzanne
Publications and source records attributed to Smrekar, Suzanne.
Science Planning for the NASA Mars Reconnaissance Orbiter Mission
The Mars Reconnaissance Orbiter (MRO), launched on August 12, 2005, carries six science instruments, each with unique requirements for repetitive global monitoring, regional or global survey mapping, and/or targeted observations of Mars. Some prefer nadir-only observations, while other instruments require many off-nadir observations (especially for stereo viewing). Because the operations requirements are often incompatible, an interactive science planning process has been developed. This process is more complex than in some recent NASA Mars missions, but less complex (and more repetitive) than processes used by many large planetary missions. It takes full advantage of MRO's novel onboard processing capabilities, and uses simple electronic interactions between geographically distributed teams. This paper describes the process used during MRO's Primary Science Phase (PSP) to plan both interactive and non-interactive observations of Mars, and what has already been learned in the tests and rehearsals preparing for PSP.
Mars Reconnaissance Orbiter (MRO): The Next Step in Mars Exploration
This slide presentation reviews the Mars Reconnaissance Orbiter (MRO), and the science strategy that motivates the exploration of Mars. The MRO is one of several missions that are planned to enhance our understanding of the planet. Included in this presentation is a review of the schedule for the MRO, the science objectives of the mission, the payloads that ae planned for MRO, and the hoped for science that will be attained from them. A review of the mission, from launch to the primary science relay is reviewed and an overview of the orbiter is shown. The presentation details the payloads, and the expected data from the instruments.
Gravity-driven deformation of the crust on Venus
Intense horizontal deformation features are observed on the surface of Venus despite the apparent absence of terrestrial-style plate tectonics. High surface temperature, low erosion rate, and regions of elevated terrain suggest that gravity spreading may be responsible for some of these features. Gravity spreading on the Earth is known to cause extensive deformation in certain thin-skinned tectonic regions, where the uppermost layers become detached along a decollement. While the high pore pressures and soft sedimentary rocks frequently observed along decollements on the Earth are not plausible for Venus, temperature induced regions of ductile deformation may exist. Simple viscous models of gravity spreading above a ductile region of the crust are developed to examine the effects of rheology, thermal gradient, surface slope and crustal thickness on deformation. For a reasonable range of parameters, the models show that surface-slope-driven ductile deformation at relatively shallow depths in the crust is possible and may be capable of detaching the uppermost rigid portion of the crust, resulting in horizontal translation.